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The Geology of the Lower Shire–Zambezi Area1

Published online by Cambridge University Press:  01 May 2009

F. Dixey
Affiliation:
Director of Geological Survey of Nyasaland.

Extract

The area lying between the Lower Zambezi and its northern tributary the Lower Shire forms a relatively small salient between the better-known parts of Portuguese East Africa lying to the north and to the south, and a study of its geology in relation to that of the larger territory has yielded interesting results. The area described includes the southern end of the Nyasaland Protectorate and that part of Portuguese East Africa lying between it and the Zambezi.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1930

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Footnotes

1

Paper read before Section C (Geology) of the Brit. Assoc. Adv. Sci., S. African meeting, 1929.

References

BIBLIOGRAPHY

I. Andrew, A. R., and Bailey, T. E. G., “Geology of Nyasaland,” Q.J.G.S., lxvi (1910), pp. 189252.CrossRefGoogle Scholar
II. Anthoine, R., et, J. Dubois, “Les Grandes Lignes de la Géologie du Bassin du Zambèze dans I'Est Africain Portugais,” C.R. XIIIe Congr. Geol. Inter., 1922, p. 751.Google Scholar
III. Dixey, F. (1) “The Limestone Resources of Nyasaland,” Bull. Geol. Surv. Nyasaland, 1927.Google Scholar
Dixey, F. (2) “The Physiography of the Shire Valley,” Rep. Geol. Surv. Nyasaland, 1925.Google Scholar
Dixey, F. (3) “The Nyasaland Section of the Great Rift Valley,” Geog. Journ., lxviii (1926), pp. 117–40.CrossRefGoogle Scholar
Dixey, F. (4) “The Dinosaur Beds of Lake Nyasa,” Trans. Roy. Soc. S. Africa, xvi, pt. i, pp. 5566. See also S. H. Haughton, op. cit., pp. 67–75.Google Scholar
Dixey, F. (5) “The Mlanje Mountains of Nyasaland,” Geog. Rev., xvii (1927), pp. 611–26.CrossRefGoogle Scholar
Dixey, F. (6) “The Lupata Gorge on the Lower Zambezi,” Geog. Journ., lxxii (1928), pp. 454–5.CrossRefGoogle Scholar
Dixey, F. (7) and Smith, W. Campbell, “The Rocks of the Lupata Gorge and the North Side of the Lower Zambezi,” Geol. Mag., LXVI (1929), pp. 241–59.CrossRefGoogle Scholar
Dixey, F. (8) “The Karroo of the Lower Shire-Zambezi Area” and “A Provisional Correlation of the Karroo North of the Zambezi,” read before XV Inter. Geol. Congr., Pretoria, 1929.Google Scholar
Dixey, F. (9) Ann. Rep. Geol. Surv. Nyasaland, 1928.Google Scholar
IV. Holmes, A., “The Pre-Cambrian and Associated Rocks of the District of Mozambique,” Q.J.G.S., lxxiv (1919), p. 31.Google Scholar
V. Mennell, F. P. (1) Trans. Geol. Soc. S. Africa, xxii (1920), p. 68.Google Scholar
Mennell, F. P. (2) “The Northward and Eastward Extension of the Karroo Lavas,” Geol. Mag., LIX (1922), pp. 166–70.CrossRefGoogle Scholar
VI. Parkinson, P. (1) “Metamorphosed Sediments in British East Africa,” Q.J.G.S., lxix (1913), pp. 534–9.CrossRefGoogle Scholar
Also (2) Parkinson, J., and Glenday, V. G., Q.J.G.S., lxxxii (1926), pp. 586614,Google Scholar
and (3) Parkinson, J., and Glenday, V. G., lxxxiii (1928), pp. 790800.Google Scholar
VII. Shand, S. J., “The Geology of Pilansberg in the Western Transvaal: A Study of Alkaline Rocks and Ring-Intrusions,” Trans. Geol. Soc., S. Africa, xxxi (1928), pp. 97156.Google Scholar
VIII. Teale, E. O. (1) “Further Notes on the Geology of Portuguese East Africa, between the Zambezi River and the Sabi River,” Geog. Journ., xlvi (1915), pp. 276–86.Google Scholar
Teale, E. O. (2) “The Geology of Portuguese East Africa between the Zambezi and Sabi Rivers,” Trans. Geol. Soc. S. Africa, xxvi (1923), p. 103.Google Scholar
IX. Teale, E. O., and Campbell-Smith, W., “Nepheline-bearing Lavas and Intrusive Rocks from South of the Zambezi,” Geol. Mag., LX (1923), pp. 226–37.CrossRefGoogle Scholar
X. Teale, E. O., and Wilson, R. C., “Portuguese East Africa between the Zambezi River and the Sabi River,” Geog. Journ., xlv (1915), pp. 1845.Google Scholar